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Acoustic noise interferometry in a time-dependent coastal ocean
1Department of Physics, Naval Postgraduate School, 833 Dyer Road, Monterey, California 93943-5216, USA.
Acoustic noise interferometry can map ocean features without sound sources. Environmental changes limit high-frequency analysis, but this limitation reveals ocean dynamics, aiding passive acoustic remote sensing.
Area of Science:
- Oceanography
- Acoustics
- Geophysics
Background:
- Passive acoustic interferometry uses ambient noise to probe ocean properties.
- Coastal ocean environments exhibit temporal variability affecting noise analysis.
- Green's functions retrieval from noise requires significant averaging times.
Purpose of the Study:
- To develop a theory quantifying environmental nonstationarity effects on noise cross-correlations.
- To understand frequency limitations in acoustic noise interferometry due to ocean variability.
- To explore the potential of coherence loss in passive acoustic remote sensing.
Main Methods:
- Theoretical development of nonstationarity effects on two-point correlation functions.
- Analysis of diffuse noise cross-correlations.
- Comparison of theoretical predictions with experimental data from the Florida Straits.
Main Results:
- Ocean temporal variability imposes an upper limit on the usable frequency range for Green's function approximation.
- Theoretical predictions align quantitatively with experimental results.
- Coherence loss at high frequencies restricts passive acoustic remote sensing to lower frequencies, impacting inversion resolution.
Conclusions:
- Environmental nonstationarity is a key factor limiting passive acoustic remote sensing resolution.
- The observed coherence loss contains valuable information on unresolved ocean dynamics.
- Passive acoustic remote sensing can be enhanced by understanding and utilizing coherence loss.
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